A Simulation and Validation of CLM during Freeze-Thaw on the Tibetan Plateau

Figure 10

Diurnal variations of soil temperature in the 10 cm soil layer in four freeze-thaw stages in the ZS site. (a) Completely frozen, (b) thawing, (c) completely thawed, and (d) freezing.

(a)

(b)

(c)

(d)